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Ceramics Division
Robert B. Sosman
B.Sc., Ohio State University, 1903Ph.D., M.I.T., 1907 (1st yr.; 1 of 3)Arthur D. Little, 1906-1908Geophysical Laboratory, 1908-1928U.S. Steel Corp., 1928-1947Rutgers University, 1947-1962The Properties of Silica, 1927; The Phases of Silica, 1965Hiker, 7th to complete Appalachian Trail (Maine-Georgia)Dancer & Dining, Gustavademecum for the Island of Manhattan
Physical ChemistPresident, The American
Ceramic Society, 1937–38Edward Orton Jr. Lecturer, 1937Albert V. Bleininger Award, 1953Ross C. Purdy Award, 1957John Jeppson Medal, 1960
James B. Austin, Proc. Geological Society of America, 251-258 (1968).
1881-1967
Edwin R. Fuller, Jr.National Institute of Standards and Technology
Gaithersburg, MD 20899-8522, U.S.A.
Microstructural Stresses:Networks, Structural Reliability,
& Antiquity Preservation
Robert B. Sosman Memorial Lecture106th Annual Meeting of
The American Ceramic SocietyIndianapolis, IN - April 21, 2004
Ceramics Division
Predict Reliability ofCeramic-Containing Components
Kovar contactKovar washer
Alumina
Kovar sleeve
Header
Ag braze
residual stresses can cause spontaneous microcracking and influence R-curve behavior & crack propagation under applied loads
Venkata R. Vedula, Shekhar Kamat & S. Jill Glass, Sandia National Laboratories
thermal expansionmismatch
thermal expansion anisotropy
Residual Stresses due to:
-
+
0
-
+
0
Ceramics Division
Thermal Degradation of Decorative Marbles
Thomas Weiß and Siegfried Siegesmund, Universität Göttingen, Germany
bowing of façade claddings (library,
Universität Göttingen)
granulardisintegrationoriginal
after 6 years
Ceramics Division
Preservation of Antiquity ArtifactsJewish cemetery in Hamburg Altona (marble tombstones)
Siegfried Siegesmund, Thomas Weiß & Joerg Ruedrich, Universität Göttingen, Germany
Harp Player (marble)Early Cycladic
2700-2300 B.C.Getty Conservation Institute
museum, Los Angeles
Ceramics Division
Microstructural Stresses
to elucidate the influence of various types of texture on microstructural residual stresses and related ensemble physical behavior and properties of polycrystalline ceramics
Objective:
Contents:Residual-Stress Networks
in Polycrystalline CeramicsMicrostructural Finite-Element AnalysisStatistical Description
of Microstructure and TextureResidual Stress and
Physical Property SimulationsThe Old and the New
Ceramics Division
Origin ofMicrostructural Stresses
Internal microstructural stresses arise due to Thermal Expansion Anisotropy (TEA) misfit between adjacent grains uponheating or cooling
-6 ppm/K
26 ppm/K
-6 ppm/K
calcite
Ceramics Division
Thermal Expansion AnisotropyMisfit Strains in a Microstructure
Cooling from strain-free temperature
Ceramics Division
Thermal Expansion AnisotropyMisfit Strains in a Microstructure
¤ Microstresses are independent of grain size ¤
Cooling from strain-free temperature
<G> = 36 µm
100 µm
Grain Orientations from EBSDelectron beam
Ceramics Division
Kikuchi bands
Electron Back-
Scattered Diffraction
500 µm
Grain Orientations from EBSDelectron beam
Ceramics Division
Kikuchi bandsalumina
Electron Back-
Scattered Diffraction
measure with piezo-or micro-Raman spectroscopy
Ceramics Division
Calculation of Microstructural Residual Stresses
Microstructure
Thermoelastic PropertiesC11, C12, C13, C33, C14, C44α11, α33
microstructural finite element
analysisGrain Orientations
EBSP
EBSD
Microstructural Residual Stresses
Ceramics Division
Stress Networks in Alumina
V.R. Vedula, S.J. Glass, D.M. Saylor, G.S. Rohrer, W.C. Carter, S.A. Langer, and E.R. Fuller, Jr., J. Am. Ceram. Soc., 84 [12], 2947-2954 (2001).
untextured EBSDmicrostructure
Grain Normals
Residual Stress Distribution upon cooling by 1500°C
Max. PrincipalStress (MPa)
Ceramics Division
Residual Stress Distribution in Untextured Alumina (∆T = -1500°C)
EBSDmicrostructure
HydrostaticStress (MPa)
Max. PrincipalStress (MPa)
Contents:
Ceramics Division
Microstructural Stresses
Contents:Residual-Stress Networks
in Polycrystalline CeramicsMicrostructural Finite-Element AnalysisStatistical Description
of Microstructure and TextureResidual Stress and
Physical Property SimulationsThe Old and the New
Microstructural Finite-Element Analysis
Ceramics Division
5 µm
NiO
ZrO2
Fe2TiO5
10 µm
Bimodal Si3N4
Material Microstructures: Heterogeneous & Stochastic
Air-Plasma-SprayedThermal Barrier Coating
Ceramics Division
Public domain software to simulate and elucidate macroscopic properties of complex materials microstructures
http://www.ctcms.nist.gov/oof
Object Oriented FiniteElement Analysis
for Materials Science and Engineering
1999 Technologies of the Year Award
Ceramics Division
Building a Microstructural ModelSimulationsExperiments
Visualization of Microstructural Physics
Virtual ParametricExperiments
Effective MacroscopicPhysical Properties
FundamentalMaterials Data
MaterialsPhysics
Microstructure Data(micrographs)
easy-to-use Graphical User Interface (GUI) – ppm2oof
Object StructureIsomorphic to the Material
Finite Element Solver
easy-to-use Graphical User Interface (GUI) – oof
Ceramics Division
Finite Element Analysis of Real Microstructuresa tool for materials scientists
to design and analyze advanced materials
ppm2oof: a tool to convert a micrograph or image of a complex, heterogeneous microstructure into a finite element mesh with constitutive properties specified by the user.
Point, Click,and SpecifyProperties
Real ( orSimulated)
Microstructure
oof: a tool to perform virtual experi-ments via finite element analysis to elucidate microstructural properties and macroscopic behavior.
Visualize andQuantifyVirtual Test
δT
oof2abaqus: converts PPM2OOF or OOF data files into input files for ABAQUS™.
Ceramics Division
Convert micrograph to “.ppm” (portable pixel map) fileSelect & identify phases to create segmented imageAssign constitutive physical properties to each phaseMesh in PPM2OOF via “Simple Mesh” or “Adaptive Mesh” – multiple algorithms that allow elements to adapt to the microstructure
PPM2OOF Tool
Segmented Image Mesh
Micrograph
Ceramics Division
Adaptive Meshing by Components
pixel imagewith mesh
mesh
pixelimage
Generate a finite-element meshfollowing the material boundaries
Ceramics Division
Eshape = 0
Eshape → 1
Ehom. > 0
Ehom. = 0
Adaptive Meshing by Components: refine elements and move nodes via Monte Carlo
annealing to reduce E = (1-α)Eshape + αEhomogeneity
createmesh
swap worstto reduce E
anneal toreduce Eimage
Ceramics Division
OOF Tool
Perform virtual experiments on finite-element mesh:To determine effective macroscopic propertiesTo elucidate parametric influencesTo visualize microstructural physics
Visualize & Quantify:Heat Flux Distribution
Virtual Experiments:Temperature Gradient
To - δT
To + δT
OOF 2.0 Current Development EffortStephen A. Langer, Andrew C. E. ReidSeung-Ill Haan, and Edwin Garcia
Ceramics Division
• Ψ = fEquil. Eq.:Ψ = Σ c • φConstitutive Eq.:
Extensible and more flexible platformEnhanced image analysis toolsExpanded element typesGeneralized constitutive relations (elasticity, piezoelectricity, etc.) w/coupling between fields
Linear and nonlinear solvers with automatic mesh refinement
– ppm2oof and oof are now combinedPlanned Additions
3-dimensional finite element solverTime-dependent solver Plasticity
Ceramics Division
Development TeamOOF
Edwin Garcia
Andrew Reid
Steve Langer Seung-Ill Haan
Craig Carter
Contents:
Ceramics Division
Microstructural Stresses
Contents:Residual-Stress Networks
in Polycrystalline CeramicsMicrostructural Finite-Element AnalysisStatistical Description
of Microstructure and TextureResidual Stress and
Physical Property SimulationsThe Old and the New
Statistical Descriptionof Microstructure and Texture
Ceramics Division
Statistical Descriptionof Microstructure
Microstructure Descriptor: h = {c, φ, g, …}• composition: c• phase: φ• crystal orientation: g = {ϕ1, Φ, ϕ2}
Microstructure Statistics• 1-point statistics: f1(h)• 2-point statistics: f2(h, h’ | r )
Grain-Boundary Statistics: S(∆g, n)
rg
sampleaxes
crystalaxes
adapted fromSurya R Kalidindi
Ceramics Division
Types of TextureCrystallographic Textureo Orientation Distributions Functions (ODF) of
grains: g = {ϕ1, Φ, ϕ2}• Random in Euler Space (uniform)
• March-Dollase Fiber Texture
• Others ODF’so Intercrystalline Misorientation Distributions
Functions (MDF): uniform and high & lowo Orientation Correlation Functions (k-point
statistics)Grain-Shape Morphologic Texture
ϕ1 ∈ {0, 2π}cos[Φ] ∈ {-1, 1}
ϕ2 ∈ {0, 2π}
f(M,θ) = M/[cos2(θ) + M sin2(θ)]3/2
M: max. MRD
θ
Ceramics Division
UniformCrystallographic Texture
15105
45
13575
165
ODF
0 30 60 90 120 150 180
uniform
Ceramics Division
Types of Misorientation Texture
0 30 60 90
low
15
105
45
135
75
1653060 90 30 60 90
0 30 60 90
uniform
0 30 60 90
high
MDF
∆θ:
15
105
45
135
75
16590 60 90 60 90 30∆θ:
15
105
45
135
75
1653030 60 30 60 90∆θ:
Contents:
Ceramics Division
Microstructural Stresses
Contents:Residual-Stress Networks
in Polycrystalline CeramicsMicrostructural Finite-Element AnalysisStatistical Description
of Microstructure and TextureResidual Stress and
Physical Property SimulationsThe Old and the New
Residual Stress and Physical Property Simulations
Ceramics Division
Simulation Model Microstructure
3-D:422 grains1003 voxels
2-D:924 grains
10002 pixels
Grains:same composition: either calcite, dolomite, or aluminasame thermoelastic properties
Orientations:different crystallographic orientations for all grainsrandom or c-axis textured distribution of crystalline orientationsuniform, and high and low distribution of intergranular misorientations
Ceramics Division
Microstructure Crystallography
Intergranular Misorientation Distributions:
Crystalline Orientations Distributions:
freq
.
0.0
0.1
0.2
0.3
0 15 30 45 60 75 90θ(°)
“low”
freq
.
0.3
0.0
0.1
0.2
0 15 30 45 60 75 90θ(°)
“uniform”
freq
.0.0
0.1
0.2
0.3
0 15 30 45 60 75 90θ(°)
“high”
Max MRD = 8
8.0
0.0
4.0
MRDMax MRD = 20
20
0
10
MRDMax MRD = 1
1.1
0.9
1.0
MRD
Ceramics Division
Phenomena Influencedby Texture
Microstructural Residual StressesElastic Strain Energy Density (a measure of microcracking propensity)Anisotropy in Bulk Thermal Expansion CoefficientAnisotropy in Bulk
Elastic ModulusMicrocracking and
its influence on properties
0 200 400 600 800 1000 1200 1400
Temperature / °C
260
280
300
320
340
360
380
400
Youn
g's M
odul
us /
GPa
heating
cooling: heating: cooling
S. Galal Yousef & J. RödelT U Darmstadt
Ceramics Division
Influence of Grain Misorientation
Distribution Functionfor a random grain orientation
distribution function
on residual stresses in polycrystalline calcite upon
heating by 100 ºC
maximum principal stress for a random grain orientation distribution function
Ceramics Division
random grain orientation distribution function
Influence of Grain Misorientation
Distribution Function
low-angle GB’suniform
high-angle GB’s
400 MPa0
35.3 ± 1.0 kJ/m3
32.3 ± 1.9 kJ/m3
23.7 ± 2.4 kJ/m3
Ceramics Division
Calcite Results
Maximum Principal Stress upon heating +100ºC for 5 random orientation distributions of calcite grains
MDF
Low
Unifo
rm#1 #2 #3 #4 #5
High
ODF:5 replications
Ceramics Division
Alum
ina Results
Maximum Principal Stress upon cooling 1500ºC for 5 random ODF‘s orientation distributions of alumina grains
MDF
Unifo
rmLo
wHigh
#1 #2 #3 #4 #5ODF:5 replications
Ceramics Division
Elastic Strain Energy Density
K (GPa)
∆α • ∆T (ppm)∆α = α3 − α1
<Elast
ic E
nerg
y Den
sity
> (k
J/m
3 ) 5 replications ODF:random(MRD=1)
MDF:o higho uniformo low
76
32 • 100
99
20 • 100
251
0.75 • 1500
Ceramics Division
Normalized Elastic Energy DensityN
orm
aliz
ed <E
last
ic E
nerg
y D
ensi
ty>
W/K
•(∆
α•∆
T)2
K (GPa)76 99 251∆α • ∆T (ppm)32 • 100 20 • 100 0.75 • 1500
ODF:random(MRD=1)
MDF:o higho uniformo low
Ceramics Division
Types of Thermal Expansion
Carrara (Italy)Carrara (Italy) Kauffung (Poland)Kauffung (Poland)Carrara (Italy)Carrara (Italy)
Ceramics Division
<CTE
> (1
0-6 /
K)Bulk Coefficient of Thermal Expansion
4.67
12.67
8.87
<α> = (2α1+α3)/3
αx αy αx αy αx αy
5 replications ODF:random(MRD=1)
MDF:o higho uniformo lowy
x
Ceramics Division
Normalized Bulk CTECT
E /<
α>
<α> = (2α1+α3)/3MRD = 1MDF:o higho uniformo low
αx αy αx αy αx αy
y
x
Ceramics Division
Venkata R. Vedula, Edwin R. Fuller, Jr. , and S. Jill Glass
Hydrostatic Stress, (σ11 + σ22), for ∆T = -1500 °C
Residual Stresses in Aluminawith Crystallographic Textured
+567
+300
+ 33
-234
-501
-767
Untextured (MRD=2)
+532
+299
+ 66
-167
-401
-635
Textured (MRD=90)
MDF:o higho uniformo low
Ceramics Division
Elastic Strain Energy Densityfor textured calcite heated +100°C
<Elast
ic E
nerg
y Den
sity
> (k
J/m
3 )
ODF: MRD
texture c-axis along y-axis
texturedrandom
texturedrandom
MDF:o higho uniformo low
<CTE
> (1
0-6 /
K)
ODF: MRD
αx
αy
αx
αy
αx
αy isotropic <α> = (2α1+α3)/3= 4.67
Ceramics Division
Bulk Thermal Expansion Anisotropyfor textured calcite heated +100°C
texture c-axis along y-axis
Ceramics Division
3-D Simulations: Elastic Energy Density
1
20
MDF“high” “low”
EED
(kJ/
m3 )
100
0
49 kJ/m3
41 kJ/m3
50 kJ/m3
18 kJ/m3
alumina cooled by 1000°C
ODF
(max
MRD
)
Ceramics Division
3-D Simulations: Elastic Energy Density
1
20
MDF“high” “low”
EED
(kJ/
m3 )
100
0 alumina cooled by 1000°C
ODF
(max
MRD
)
isosurfaces for energy density > 100 kJ/m3
Ceramics Division
Elastic Strain Energy Densityfor textured alumina cooled 1000°C
<Elast
ic E
nerg
y Den
sity
> (k
J/m
3 )
MDF:o higho uniformo low
ODF: MRD
3 replications
texturedrandom
texture c-axis along y-axis
Ceramics Division
Bulk Thermal Expansion Anisotropyfor textured alumina cooled 1000°C
MDF:o higho uniformo low
<CTE
> (1
0-6 /
K)
ODF: MRD
α⊥
αll
α⊥
αll
α⊥
αll
isotropic <α> = (2α1+α3)/3= 8.87
3 replications
texturedrandom
texture c-axis along y-axis
What is a good metric for characterizingresidual-stress isosurfaces?
Ceramics Division
Residual-Stress Isosurfaces
e.g., isosurface of elastic energy densities greater than 100 kJ/m3
homology groups and topological invariants — measure the topological complexity of objects in any dimension.
Thomas Wanner, George Mason University, proposed the use of:
Ceramics Division
Residual-Stress Isosurfaces
e.g., isosurface of elastic energy densities greater than 100 kJ/m3
Ceramics Division
Computational Algebraic Topology
CHomP (Computational Homology Program): pixel/voxel oriented public-domain software for computing algebraic topological invariants. Associated New Textbook: Computational Homology by Tomasz Kaczynski, Konstantin Mischaikow , and Marian Mrozek, (Applied Mathematical Sciences , Vol. 157, Springer-Verlag, 2004).
Challenge in Computational Algebraic Topology:Theoretically, determination of homology groups and topological invariants is straightforward.Computationally, such determination may be intractable or infeasible for large data sets.
Algebraic Topology:a branch of mathematics, in which tools from abstract algebra are used to study topological spaces.
Ceramics Division
Topological Invariants of Space
Topological Invariants of a Complex ObjectBetti numbers, named for Enrico Betti, are a sequence β0, β1, ... of topological invariants, which are natural numbers, or infinity.Other invariants include: torsion coefficientsand the Euler characteristic.
Homology groups: a more general measure of the complexity of the object in any dimension.
… invariant under transformations that do not require cutting or gluing of the object.
Ceramics Division
Zeroth Betti NumbersBetti number β0 counts the number of connected components of the structure
How many distinct connected regions does the maze have?
Computational Homology, Applied Mathematical Sciences , Vol. 157, Springer-Verlag, 2004).
Ceramics Division
Zeroth Betti NumbersBetti number β0 counts the number of connected components of the structure
Computational Homology, Applied Mathematical Sciences , Vol. 157, Springer-Verlag, 2004).
Cut along the blue lines: the zeroth Betti number is the number of pieces that the maze falls apart into.
Ceramics Division
First Betti NumberBetti number β1 counts the number of independent tunnels created by the structure: the number of loops in the structure that cannot be
shrunk to a point, ormorphed into each other.
β1 = 0 β1 = 2
β1 = 4
Ceramics Division
Second Betti NumberBetti number β2 counts the number of
closed regions created by the structure.
all surfaces have β2 = 1
Ceramics Division
Max. Principal Stress Networks
Thomas Wanner, George Mason UniversityKonstantin Mischaikow, Georgia Institute of Technology
isosurface forσ1 > 201 MPa
β2
β1
β0
Threshold Level for Max. Principal Stress
Bett
i num
ber
Ceramics Division
Max. Principal Stress Networks
Thomas Wanner, George Mason UniversityKonstantin Mischaikow, Georgia Institute of Technology
isosurface forσ1 < 27.5 MPa β2
β1
β0
Threshold Level for Max. Principal Stress
Bett
i num
ber
Contents:
Ceramics Division
Microstructural Stresses
Contents:Residual-Stress Networks
in Polycrystalline CeramicsMicrostructural Finite-Element AnalysisStatistical Description
of Microstructure and TextureResidual Stress and
Physical Property SimulationsMonument RestorationThe Old and the New
The Tomb of the Unknowns
Ceramics Division
Made from a 55-ton block of white marble from the Yule Marble Quarry located near Marble, Colorado, the monument was dedicated in 1932.
A crack, first discovered in the 1940’s during the Truman administration, has continued to grow.
Unknowns Monument Will Be ReplacedBy Annie Gowen, The Washington Post, Monday, May 26, 2003, B01
“The growing crack that now circles the marble monument has split the three figures representing Peace, Victory and Valor.”
(James A. Parcell - The Washington Post)
“Officials decided to replace the stone after concluding that a 1989 cosmetic repair job — which cemetery historian Thomas Sherlock compared to fixing a bathtub with tile grout — had done nothing to conceal the problem and may have exacerbated it.”
Ceramics Division
Microstresses are independent of grain size
Residual Stressesin Nanostructured Ceramics
Ceramics Division
Residual Stressesin Nanostructured Ceramics
Ceramics Division
new phenomena (physics) at the small-scale? e.g., surface stresses: σij = γ δij + (∂γ/∂εij)
Residual Stressesin Nanostructured Ceramics
Ceramics Division
100 µm
6 µm
new phenomena (physics) at the small-scale? e.g., surface stresses: σij = γ δij + (∂γ/∂εij)
Ceramics Division
Collaborators & AcknowledgmentsStephen A. Langer, Information Tech. Lab, NISTAndrew C. E. Reid, Edwin Garcia, & Seung-Ill Haan, MSEL, NISTW. Craig Carter, MITDavid M. Saylor, U.S. Food and Drug AdministrationEdward Lin, Montgomery Blair High SchoolThomas Weiß & Siegfried Siegesmund, Geowissenschaftliches Zentrum der Universität Göttingen, GermanyThomas Wanner, George Mason UniversityAndré Zimmermann, Bosch GmbH, GermanySusan Galal Yousef & Jürgen Rödel, Technische Universität Darmstadt, GermanyVenkata R. Vedula, Shekhar Kamat, Raj Tandon, Saundra Monroe, S. Jill Glass & Clay Newton, Sandia Natl. LabsChang-Soo Kim & Gregory S. Rohrer, Carnegie Mellon UniversityAlbert Paul and Grady White, MSEL, NISTBarbara Fuller
Ceramics Division
AbstractMicrostructural Stresses: Networks, Structural
Reliability, & Antiquity PreservationEdwin R. Fuller, Jr.
National Institute of Standards and Technology,Gaithersburg, Maryland 20899-8522, U.S.A.
Macroscopic behavior and ensemble physical properties of heterogeneous materials, such as polycrystalline ceramics or stone, depend on the thermoelastic properties of the constituent phases, their morphology, and their topology. Or simply, on the crystallites, their shape, and how they are arranged. Because crystalline properties are typically anisotropic, this dependence encompasses the distribution of crystallite orientations (crystallographic texture) as well as distributional aspects of crystallite shape and spatial arrangements. A property profoundly affected by these heterogeneous and stochastic features is the internal, or microstructural stresses. Their influence on behavior can be either deleterious, as in performance degradation of ceramic components or physical deterioration of stone sculptures and monuments, or advantageous, as in transformation and grain-bridging toughening phenomena. Microstructural stresses occur from many causes: temperature changes in conjunction with thermal expansion differences between features, phase transformations, or crystallization of fluids or salts in pores (e.g., freeze/thaw cycles). Many materials science tools are available to elucidate these phenomena. Computational materials science, however, provides a particularly facile means for examining material response to a wide variety of physical conditions. A recently observed phenomenon in polycrystalline materials with crystalline thermal expansion anisotropy is the development of residual-stress networks upon cooling or heating. Moreover, the length-scale of these networks encompasses many grains. To study this and related phenomena, two- and three-dimensional model microstructures were generated with a pixel/voxel-based tessellation technique that constructs grains whose morphologies conform to a predefined statistical distribution. Crystal orientations were overlaid on the grain structure such that grain orientation and misorientation distribution functions also match predefined statistical distributions. Microstructure-based finite-element simulations were then used to elucidate the origin of the residual stress networks, and to characterize the influence of texture on network size and associated polycrystalline physical properties, such as bulk thermal expansion and microcracking propensity.